SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 35:776-780 (1971)
© 1971 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Frazier, B. E.
Right arrow Articles by Lee, G. B.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Frazier, B. E.
Right arrow Articles by Lee, G. B.
Agricola
Right arrow Articles by Frazier, B. E.
Right arrow Articles by Lee, G. B.

Characteristics and Classification of Three Wisconsin Histosols1

B. E. Frazier and G. B. Lee2

ABSTRACT

On the basis of morphology, pH, and solubility in Na4P2O7, three Wisconsin histosols were classified as (i) a Fibrist, (ii) a Hemist, and (iii) a Saprist.

Fiber content was found to be the single most useful characteristic in the classification of these Histosols, and in quantifying various stages of decomposition and soil formation in histic materials. Fibric material consisted of 70% or more fiber as determined on a gravimetric basis, using a 140 mesh sieve to separate fibrous (> 0.1 mm) from nonfibrous (< 0.1 mm) material. The fiber content of hemic material ranged from 35 to 60%; sapric material contained < 15% fiber. Sodium pyrophosphate extract color (SPEC) is a useful parameter in the characterization and classification of histic materials.

Results of other analysis showed that the carbon content of the organic fraction was highest in the Saprist and lowest in the Fibrist. Oxygen and hydrogen contents were, in general, inversely related to fiber content. Total nitrogen appeared to be dependent on botanical composition of parent plants and microbial activity of the soil; the relatively high nitrogen content of certain subsurface layers may be related to illuvial deposition of mobile, nitrogen-containing substances. Mineral content was likely influenced by additional colluvial or eolian sediments.

Good structure was found in both surface and subsurface layers of the Saprist. It is suggested that highly decomposed Saprists possessing good structure in surface and subsoil horizons be placed in a separate great group.


NOTES

1 Research supported by the College of Agricultural and Life Sciences, Univ. of Wis., Madison 53706. Presented before Div. S-5, Soil Science Society of America, New Orleans, La., Nov. 1968.

2 Research Assistant and Associate Professor of Soils, respectively.

Received for publication February 25, 1971. Accepted for publication May 28, 1971.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1971 by the Soil Science Society of America.